Barium and lithium in foraminifera: glacial-interglacial changes in the North Atlantic
The trace element content of calcareous foraminifera provides a powerful tool to the study of glacial-interglacial changes in the physical and chemical properties of the ocean. Foraminifera incorporate barium in direct proportion to its concentration in seawater. Using barium as a nutrient proxy, Ba...
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LSU Digital Commons
2002
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Online Access: | https://digitalcommons.lsu.edu/gradschool_dissertations/3135 https://doi.org/10.31390/gradschool_dissertations.3135 https://digitalcommons.lsu.edu/context/gradschool_dissertations/article/4134/viewcontent/uc.pdf |